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  • 1
    Call number: ZSP-686-200
    In: Report
    Type of Medium: Monograph available for loan
    Pages: 31 S. : graph. Darst.
    ISSN: 0937-1060
    Series Statement: Report / Max-Planck-Institut für Meteorologie 200
    Language: English
    Location: AWI Reading room
    Branch Library: AWI Library
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  • 2
    Call number: MOP 47908 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 94 S.
    Series Statement: ETH Greenland Expedition : progress report 2
    Location: MOP - must be ordered
    Branch Library: GFZ Library
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  • 3
    Call number: AWI A3-96-0058
    In: Zürcher geographische Schriften
    Type of Medium: Monograph available for loan
    Pages: 66 S.
    ISBN: 3728118591
    Series Statement: Zürcher geographische Schriften 44
    Branch Library: AWI Library
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  • 4
    Call number: AWI A4-92-0032
    In: Zürcher geographische Schriften
    Description / Table of Contents: Table of contents: List of figures. - List of tables. - Acknowledgement. - Introduction. - PART 1 CLIMATE ON TUNDRA. - 1 Climate of the base camp. - 2 Mesoclimate of the expedition area. - PART 2 ENERGY BALANCE ON THE TUNDRA. - 1 Radiation. - 2 Turbulent heat fluxes. - 3 Subsurface energy transfer. - 4 Latent heat of fusion. - 5 Energy balance. - 6 Regional water balance on tundra. - PART 3 SYNTHESIS. - Conclusion. - References. - Zusammenfassung. - Abstract
    Type of Medium: Series available for loan
    Pages: XX, 448 S. : Ill.
    Series Statement: Zürcher geographische Schriften 3
    Branch Library: AWI Library
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  • 5
    Call number: AWI A3-96-0057
    In: Zürcher geographische Schriften
    Type of Medium: Monograph available for loan
    Pages: III, 62 S.
    ISBN: 3728116793
    Series Statement: Zürcher geographische Schriften 34
    Branch Library: AWI Library
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Pure and applied geophysics 119 (1980), S. 259-277 
    ISSN: 1420-9136
    Keywords: intercomparison ; Radiosondes ; Statistical analysis
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract This paper describes an intercomparison between the Väisälä, VIZ and Swiss (used at upper-air station 06610) radiosondes. The field experiment was supported by a series of carefully implemented laboratory tests. The results show that the temperature sensor data from the SMI and VIZ sondes both require additional radiation compensation for daylight ascents whilst the Swiss sonde's pressure sensor has particularly large errors in the 200–100 mb region. New correction parameters have been determined for the SMI and VIZ sondes and these have now been built into the systems' software.
    Type of Medium: Electronic Resource
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  • 7
    ISSN: 1432-0894
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract The ability of a high resolution (T106) version of the ECHAM3 general circulation model to simulate regional scale surface radiative fluxes has been assessed using observations from a new compilation of worldwide instrumentally-measured surface fluxes (Global Energy Balance Archive, GEBA). The focus is on the European region where the highest density of observations is found, and their use for the validation of global and regional climate models is demonstrated. The available data allow a separate assessment of the simulated fluxes of surface shortwave, longwave, and net radiation for this region. In summer, the incoming shortwave radiation calculated by the ECHAM3/T106 model is overestimated by 45 W m−2 over most of Europe, which implies a largely unrealistic forcing on the model surface scheme and excessive surface temperatures. In winter, too little incoming shortwave radiation reaches the model surface. Similar tendencies are found over large areas of the mid-latitudes. These biases are consistent with deficiencies in the simulation of cloud amount, relative humidity and clear sky radiative transfer. The incoming longwave radiation is underestimated at the European GEBA stations predominantly in summer. This largely compensates for the excessive shortwave flux, leading to annual mean net radiation values over Europe close to observations due to error cancellation, a feature already noted in the simulated global mean values in an earlier study. Furthermore, the annual cycle of the simulated surface net radiation is strongly affected by the deficiencies in the simulated incoming shortwave radiation. The high horizontal resolution of the GCM allows an assessment of orographically induced flux gradients based on observations from the European Alps. Although the model-calculated and observed flux fields substantially differ in their absolute values, several aspects of their gradients are realistically captured. The deficiencies identified in the model fields are generally consistent at most stations, indicating a high degree of representativeness of the measurements for their larger scale setting.
    Type of Medium: Electronic Resource
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  • 8
    ISSN: 1432-0894
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract. The ability of a high resolution (T106) version of the ECHAM3 general circulation model to simulate regional scale surface radiative fluxes has been assessed using observations from a new compilation of worldwide instrumentally-measured surface fluxes (Global Energy Balance Archive, GEBA). The focus is on the European region where the highest density of observations is found, and their use for the validation of global and regional climate models is demonstrated. The available data allow a separate assessment of the simulated fluxes of surface shortwave, longwave, and net radiation for this region. In summer, the incoming shortwave radiation calculated by the ECHAM3/T106 model is overestimated by 45 W m–2 over most of Europe, which implies a largely unrealistic forcing on the model surface scheme and excessive surface temperatures. In winter, too little incoming shortwave radiation reaches the model surface. Similar tendencies are found over large areas of the mid-latitudes. These biases are consistent with deficiencies in the simulation of cloud amount, relative humidity and clear sky radiative transfer. The incoming longwave radiation is underestimated at the European GEBA stations predominantly in summer. This largely compensates for the excessive shortwave flux, leading to annual mean net radiation values over Europe close to observations due to error cancellation, a feature already noted in the simulated global mean values in an earlier study. Furthermore, the annual cycle of the simulated surface net radiation is strongly affected by the deficiencies in the simulated incoming shortwave radiation. The high horizontal resolution of the GCM allows an assessment of orographically induced flux gradients based on observations from the European Alps. Although the model-calculated and observed flux fields substantially differ in their absolute values, several aspects of their gradients are realistically captured. The deficiencies identified in the model fields are generally consistent at most stations, indicating a high degree of representativeness of the measurements for their larger scale setting.
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    Springer
    GeoJournal 8 (1984), S. 221-228 
    ISSN: 1572-9893
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geography
    Notes: Abstract Seasonal change in the energy balance on the arctic tundra is presented. The thermal stability of a dry snow cover is investigated in detail. In addition to high reflection by the snow cover, a significant absorption of solar radiation on the very surface of the snow cover was found responsible for the thermal stability. The efficient absorption of solar radiation by the surface rather than the interior of the snow cover and the almost immediate removal of the absorbed energy through radiative emission and turbulent heat fluxes keep the temperature of the snow cover low. The energy balances for the melt and postmelt period for various arctic surfaces are compared. The most important difference of the energy balance between the tundra and tther low attitude arctic surface, such as the sea and ablation areas of glaciers, is not the net radiation but the latent heat of fusion. Extremely small heat cosuumption through the melt on the tundra is the basis for higher temperature, characteristics to the tundra climate in the Arctic.
    Type of Medium: Electronic Resource
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  • 10
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    Cambridge University Press
    Publication Date: 2015-05-10
    Print ISSN: 0022-1430
    Electronic ISSN: 1727-5652
    Topics: Geography , Geosciences
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